Laserfiche WebLink
<br />For riverine, lacustrine, and coastal <br />flooding sources studied by detailed <br />methods, FEMA performs analyses of the <br />100-year flood and, usually, the 10-, SO-, <br />and SOO-year floods. Often a hydraulic <br />analysis of the 100-year floodway is <br />performed for riverine flooding sources. <br />For sheetflow and alluvial fan flooding <br />sources studied by detailed methods, <br />and for all flooding sources studied by <br />approximate methods, FEMA usually <br />performs analyses of only the 100-year <br />flood. <br /> <br />Therefore, the extent of the hydrologic <br />and hydraulic analyses that a revision <br />requestor may be required to submit is <br />determined not only by the basis of the <br />revision request, but also by the type of <br />flooding source and the scope of the <br />study on which the effective NFIP map is <br />based. <br /> <br />. Unless the revision request is based on <br />the use of alternative models or <br />methodologies, the hydrologic and <br />hydraulic analyses that the revision <br />requestor submits must be performed <br />with the models used in the preparation <br />of the effective NFIP map. For riverine <br />flooding sources studied by detailed <br />methods, the hydrologic analyses on <br />which NFIP maps are based are usually <br />performed with standard engineering <br />methodologies, such as flood-frequency <br />analyses of stream gage data, or with <br />widely accepted computer models, such <br />as the COE HEC-1 model or the SCS TR-20 <br />model. <br /> <br />The hydraulic analyses for riverine <br />flooding sources are usually performed <br />with the COE HEC-2 step-backwater <br />model or a similar and widely accepted <br />model, such as the SCS WSP-2 model or <br />the USGS WSPRO model. <br /> <br />For the analysis of alluvial fan flood <br />hazards and the hazards associated with <br />coastal storm surge and wave action, <br />including wave height and wave runup, <br />FEMA has established or adopted special <br />methodologies and computer models. <br /> <br />For detailed analyses of lacustrine and <br />sheetflow flood hazards, and for <br />approximate analyses of all types of <br />flooding sources, FEMA uses a variety of <br />standard engineering models and <br />methodologies. <br /> <br />The revision requestor may ask FEMA for <br />copies of the input and output data from <br />the model(s) used, or copies of other <br />calculations or analyses performed, in <br />the preparation of a specific NFIP map. <br />(See Appendix C.) <br /> <br />. As required by Paragraph 6S.6(a)(6) of <br />the NFIP regulations, when a revision <br />request is based on the use of an <br />alternative hydrologic or hydraulic <br />model, the requestor must show that the <br />model used has been reviewed and <br />approved for general use by a Federal <br />agency responsible for water resources <br />activities or a notable scientific body, is <br />well documented (with a user's manual <br />that includes source codes), and is <br />available to the general user (i.e., in the <br />public domain and non-proprietary). <br /> <br />. When the requestor is required to <br />submit a new model, all differences <br />between the conditions represented by <br />the original and revised models must be <br />justified by physical changes that have <br />occurred, or the use of better hydraulic <br />data or revised discharges. The new <br />model should also account for all <br />encroachments that have occurred in the <br />floodplain since the original model was <br />developed. <br /> <br />. When a hydrologic or hydraulic analysis <br />is submitted to FEMA, copies of the input <br />and output data from the original and <br />revised computer models must be <br />submitted. <br /> <br />. For information concerni ng additional <br />data that must be submitted in support <br />of requests that involve changes to <br />floodways, refer to Chapter 7. <br /> <br />. When a request for a revision to <br />floodplai n boundaries is based on data <br />that show changed topographic <br /> <br />2S <br />